RT Journal Article
T1 Indicadores estructurales y morfológicos de deformaciones postmiocenas en el sector occidental de la Falla de Crevillente (Cordillera Bética)
T1 Structural and morphological indicators of postmiocene deformations in the western Crevillente Fault (Betic Cordillera)
A1 Canora-Catalán, C.
A1 Martínez Díaz, José Jesús
AB According to the NNW-SSE regional shortening direction active in the Eastern Betic Cordillera since the Upper Miocene, the ENE-WSW Crevillente Fault should be either blocked or locally reverse. However, dextral, sinestral or reverse movements have been reported along the fault zone. In this work, new observations on the post-Miocene deformations of the Crevillente Fault are described. A block-tectonics model active on different scales is proposed to explain the kinematics variability of the fault.
PB Sociedad Geológica de España
SN 0213-683X
YR 2006
FD 2006
LK https://hdl.handle.net/20.500.14352/120281
UL https://hdl.handle.net/20.500.14352/120281
LA spa
NO Martínez Díaz, J.J. y Canora Catalán, C. (2005) «Indicadores estructurales y morfológicos de deformaciones postmiocenas en el sector occidental de la Falla de Crevillente (Cordillera Bética)», Geogaceta, 39, pp. 71-74.
DS Docta Complutense
RD 20 ene 2026